COSC-2 – drilling the basal décollement and underlying margin of palaeocontinent Baltica in the Paleozoic Caledonide Orogen of Scandinavia

IF 1.6 Q3 GEOSCIENCES, MULTIDISCIPLINARY Scientific Drilling Pub Date : 2022-02-25 DOI:10.5194/sd-30-43-2022
H. Lorenz, Jan-Erik Rosberg, C. Juhlin, I. Klonowska, R. Lescoutre, G. Westmeijer, B. Almqvist, M. Anderson, S. Bertilsson, M. Dopson, J. Kallmeyer, J. Kück, O. Lehnert, L. Menegon, C. Pascal, S. Rejkjær, Nick N. W. Roberts
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引用次数: 3

Abstract

Abstract. The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project aims to characterise the structure and orogenic processes involved in a major collisional mountain belt by multidisciplinary geoscientific research. Located in western central Sweden, the project has drilled two fully cored deep boreholes into the bedrock of the deeply eroded Early Paleozoic Caledonide Orogen. COSC-1 (2014) drilled a subduction-related allochthon and the associated thrust zone. COSC-2 (2020, this paper) extends this section deeper through the underlying nappes (Lower Allochthon), the main Caledonian décollement, and the upper kilometre of basement rocks. COSC-2 targets include the characterisation of orogen-scale detachments, the impact of orogenesis on the basement below the detachment, and the Early Paleozoic palaeoenvironment on the outer margin of palaeocontinent Baltica. This is complemented by research on heat flow, groundwater flow, and the characterisation of the microbial community in the present hard rock environment of the relict mountain belt. COSC-2 successfully, and within budget, recovered a continuous drill core to 2276 m depth. The retrieved geological section is partially different from the expected geological section with respect to the depth to the main décollement and the expected rock types. Although the intensity of synsedimentary deformation in the rocks in the upper part of the drill core might impede the analysis of the Early Paleozoic palaeoenvironment, the superb quality of the drill core and the borehole will facilitate research on the remaining targets and beyond. Protocols for sampling in the hard rock environment and subsequent sample preservation were established for geomicrobiological research and rock mechanical testing. For the former, a sparse sample series along the entire drill core was taken, while the target of the latter was the décollement. COSC-2 was surveyed by a comprehensive post-drilling downhole logging campaign and a combined borehole/land seismic survey in autumn 2021. This paper provides an overview of the COSC-2 (International Continental Scientific Drilling Project – ICDP 5054_2_A and 5054_2_B boreholes) operations and preliminary results. It will be complemented by a detailed operational report and data publication.
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斯堪地那维亚加里东构造带古生代波罗的海古大陆基底和下缘的COSC-2钻探
摘要斯堪的纳维亚加里东ides碰撞造山运动(COSC)科学钻探项目旨在通过多学科的地球科学研究来表征一个主要碰撞山带的构造和造山过程。该项目位于瑞典中西部,在早古生代加里东构造造山带的基岩上钻了两个完全取心的深钻孔。COSC-1(2014)钻探了与俯冲相关的异体及其逆冲带。COSC-2(2020,本文)将该剖面延伸至下推覆体(下Allochthon)、主要的加里东运动和上公里的基底岩石。COSC-2研究对象包括造山带尺度分离的特征、造山作用对分离下基底的影响以及波罗的海古大陆外缘早古生代古环境。在此基础上,还开展了热流、地下水流动、微生物群落特征等方面的研究。cosc -2成功地在预算范围内回收了深度为2276米的连续岩心。检索到的地质剖面与预期的地质剖面在主剖面的深度和预期的岩石类型方面存在部分差异。虽然岩心上部岩石的同沉积变形强度可能会阻碍对早古生代古环境的分析,但岩心和钻孔的优良质量将有助于对剩余目标及其他区域的研究。为地质微生物研究和岩石力学测试建立了在硬岩环境中取样和随后的样品保存的方案。对于前者,沿着整个岩心取一个稀疏的样本序列,而后者的目标是dsamement。2021年秋季,通过全面的钻井后井下测井活动和井/陆联合地震调查对COSC-2进行了调查。本文概述了COSC-2(国际大陆科学钻探项目- ICDP 5054_2_A和5054_2_B钻孔)的作业和初步结果。该报告将辅以详细的业务报告和数据出版物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Scientific Drilling
Scientific Drilling GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
2.50
自引率
0.00%
发文量
12
审稿时长
27 weeks
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